Scheelite is highly sought after by collectors for its brilliant blue fluorescence under short-wave UV light, which is a key diagnostic feature. It typically occurs as sharp bipyramidal crystals in skarn deposits formed by the contact metamorphism of limestone with igneous intrusions.
Is this scheelite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch scheelite with a known reference. Scheelite sits at Mohs 4.5-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to adamantine.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow, brownish yellow, reddish yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: columnar, disseminated, massive.
Often confused with
Scheelite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Quartz is the harder of the two (Mohs 7 vs. 4.5-5).

How to tell apart: Scheelite is noticeably harder (Mohs 4.5-5 vs. 3).

How to tell apart: Streak differs, so Scheelite leaves white, Powellite leaves light yellow; luster reads vitreous to adamantine on Scheelite and subadamantine, resinous, pearly on Powellite.
Often found alongside scheelite
Minerals reported to co-occur with scheelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaWO₄
- Mohs hardness
- 4.5-5
- Density
- 6.10 g/cm³
- Streak
- White
- Luster
- Vitreous to adamantine
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Columnar, disseminated, massive
- Cleavage
- On {101}, distinct; on {112}, interrupted; on {001}, indistinct
- Fluorescence
- Bright bluish white under SW UV
- Rarity
- Common
- Uses
- Ore of tungsten, Collector, Fluorescent specimens
- Host rock
- Typically a component of contact-metamorphic tactite; in high-temperature hydrothermal veins and greisen; less common in granite pegmatites and medium-temperature hydrothermal veins; alluvial
Where rockhounds find scheelite
20 mapped spotsClassic worldwide localities
- Cohen mine, Dragoon Mountains, Cochise Co., Arizona, USA
- Commercially mined at the Pine Creek mine, near Bishop, Inyo Co., California, USA
- Bispberg iron mine, near Säter, Dalarne, Sweden
- Altenberg and Schwarzenberg, Saxony, Germany
- Cínovec (Zinnwald) and Horní Slavkov (Schlaggenwald), Czech Republic
- Traversella, Piedmont, Italy
U.S. states with scheelite
Each link opens a state-specific list of mapped rockhounding spots that produce scheelite.
Field-hunting tip
Where it forms: Typically a component of contact-metamorphic tactite; in high-temperature hydrothermal veins and greisen; less common in granite pegmatites and medium-temperature hydrothermal veins; alluvial. If you start seeing cassiterite, wolframite, topaz in float, you are in the right ground. Typical habit: columnar, disseminated, massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Montana, North Carolina. Start trip planning there.








